风化率 meaning in Chinese
rate of creep
Examples
- Constraints on silicate weathering rates in different settings : climatic or tectonic
不同构造带硅酸盐化学风化率的制约:气候还是构造 - For the mass balance equations , the average mechanical denudation rates would be estimated based on chemical weathering rates for the major basins of china
研究发现综合岩性整体上控制了中国主要流域盆地化学风化率的大小，但化学风化率一定程度上也受制于流域岩石的化学风化进程。 - In fact , as a very important part of material geochemistry cycle , chemical weathering and mechanical denudation plays a crucial role in affecting and changing the surface continent deeply
扣除大气降水、人类活动、大气co :等非岩石风化来源的物质后得到了中国17个主要流域盆地较为准确的化学风化率数值。 - Many studies had attempted to characterize chemical weathering process by focusing on geochemisty of river particulate and sediment . the sediment geochemistry may reflect and compare with the carbonates and silicates weathering degree by introducing the chemical index of alteration ( cia ) and new sediment index of variation ( siv ) and elemental molar abundance ratio of the sediment . the one main objective of this study would provide and compare the relative weathering intensities of silicates and carbonates with the different basins
2沉积物地球化学与化学风化进程和机械剥蚀率化学风化指数与化学风化率属于表征化学风化作用意义不同的函数，前者为相对概念反映流域岩石在原岩基础上己发生淋溶作用的深度，主要受到了气候因子的深刻影响(中国流域沉积物化学风化指数由北到南呈有规则的递增序列，气候因子对风化进程的影响掩盖了岩性的巨大差异) ，而化学风化率含义是指单位流域面积岩石风化淋溶产生的离子绝对总量。